Electromagnetic Induction Measurements near Ny Alesund ...
Electromagnetic induction is a non-invasive mapping technique used in a variety of applications including geological mapping and civil engineering, agriculture and forestry, environmental monitoring, groundwater protection, mineral exploration and archaeology. Electromagnetic induction is mainly use...
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Online Access: | https://dx.doi.org/10.5281/zenodo.8289452 https://zenodo.org/doi/10.5281/zenodo.8289452 |
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ftdatacite:10.5281/zenodo.8289452 2024-01-28T10:08:33+01:00 Electromagnetic Induction Measurements near Ny Alesund ... Uta Koedel Claudia Schuetze Peter Dietrich 2023 https://dx.doi.org/10.5281/zenodo.8289452 https://zenodo.org/doi/10.5281/zenodo.8289452 en eng Zenodo https://dx.doi.org/10.5281/zenodo.8289451 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Polar MOSES AWIPEV Ny Alesund/Svalbard Geophysics FOS Earth and related environmental sciences Electromagnetic Induction EMI Long term observatory Bayelva 2023_MOSES_PolarMOSES Dataset dataset 2023 ftdatacite https://doi.org/10.5281/zenodo.828945210.5281/zenodo.8289451 2024-01-04T22:10:18Z Electromagnetic induction is a non-invasive mapping technique used in a variety of applications including geological mapping and civil engineering, agriculture and forestry, environmental monitoring, groundwater protection, mineral exploration and archaeology. Electromagnetic induction is mainly used to measure the (apparent) electrical conductivity of the subsurface, which depends on various soil properties such as clay content, water content and salinity. The nature and strength of the relationships between electrical conductivity and soil properties are site-specific. The instrument used, the EM38-MK2, measures both the quadrature (conductivity) and the inphase (magnetic susceptibility) components at two different depths, all at the same time, without the need for ground contact. The aim of the measurements was to improve the understanding of thaw-driven landscape dynamics in permafrost regions and to assess the vulnerability of permafrost to thaw. The measurements were carried out in August 2023 in the ... Dataset permafrost Svalbard DataCite Metadata Store (German National Library of Science and Technology) Bayelva ENVELOPE(11.898,11.898,78.933,78.933) Moses ENVELOPE(-99.183,-99.183,-74.550,-74.550) Svalbard |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
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language |
English |
topic |
Polar MOSES AWIPEV Ny Alesund/Svalbard Geophysics FOS Earth and related environmental sciences Electromagnetic Induction EMI Long term observatory Bayelva 2023_MOSES_PolarMOSES |
spellingShingle |
Polar MOSES AWIPEV Ny Alesund/Svalbard Geophysics FOS Earth and related environmental sciences Electromagnetic Induction EMI Long term observatory Bayelva 2023_MOSES_PolarMOSES Uta Koedel Claudia Schuetze Peter Dietrich Electromagnetic Induction Measurements near Ny Alesund ... |
topic_facet |
Polar MOSES AWIPEV Ny Alesund/Svalbard Geophysics FOS Earth and related environmental sciences Electromagnetic Induction EMI Long term observatory Bayelva 2023_MOSES_PolarMOSES |
description |
Electromagnetic induction is a non-invasive mapping technique used in a variety of applications including geological mapping and civil engineering, agriculture and forestry, environmental monitoring, groundwater protection, mineral exploration and archaeology. Electromagnetic induction is mainly used to measure the (apparent) electrical conductivity of the subsurface, which depends on various soil properties such as clay content, water content and salinity. The nature and strength of the relationships between electrical conductivity and soil properties are site-specific. The instrument used, the EM38-MK2, measures both the quadrature (conductivity) and the inphase (magnetic susceptibility) components at two different depths, all at the same time, without the need for ground contact. The aim of the measurements was to improve the understanding of thaw-driven landscape dynamics in permafrost regions and to assess the vulnerability of permafrost to thaw. The measurements were carried out in August 2023 in the ... |
format |
Dataset |
author |
Uta Koedel Claudia Schuetze Peter Dietrich |
author_facet |
Uta Koedel Claudia Schuetze Peter Dietrich |
author_sort |
Uta Koedel |
title |
Electromagnetic Induction Measurements near Ny Alesund ... |
title_short |
Electromagnetic Induction Measurements near Ny Alesund ... |
title_full |
Electromagnetic Induction Measurements near Ny Alesund ... |
title_fullStr |
Electromagnetic Induction Measurements near Ny Alesund ... |
title_full_unstemmed |
Electromagnetic Induction Measurements near Ny Alesund ... |
title_sort |
electromagnetic induction measurements near ny alesund ... |
publisher |
Zenodo |
publishDate |
2023 |
url |
https://dx.doi.org/10.5281/zenodo.8289452 https://zenodo.org/doi/10.5281/zenodo.8289452 |
long_lat |
ENVELOPE(11.898,11.898,78.933,78.933) ENVELOPE(-99.183,-99.183,-74.550,-74.550) |
geographic |
Bayelva Moses Svalbard |
geographic_facet |
Bayelva Moses Svalbard |
genre |
permafrost Svalbard |
genre_facet |
permafrost Svalbard |
op_relation |
https://dx.doi.org/10.5281/zenodo.8289451 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.5281/zenodo.828945210.5281/zenodo.8289451 |
_version_ |
1789337452410830848 |